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Cited by 1,206

The DOI matches its Crossref record; 17 of the 17 references it cites were found in a registry or an index.

Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas event

Open access
Alley, R. B., Meese, D. A., Shuman, C. A., Gow, A. J., Taylor, K. C., Grootes, P. M., White, J. W. C., Ram, M., Waddington, E. D., Mayewski, P. A., Zielinski, G. A.·1993·Nature

Abstract

THE warming at the end of the last glaciation was characterized by a series of abrupt returns to glacial climate, the best-known of which is the Younger Dryas event1. Despite much study of the causes of this event and the mechanisms by which it ended, many questions remain unresolved1. Oxygen isotope data from Greenland ice cores2–4 suggest that the Younger Dryas ended abruptly, over a period of about 50 years; dust concentrations2,4 in these cores show an even more rapid transition (≲20 years). This extremely short timescale places severe constraints on the mechanisms underlying the transition. But dust concentrations can reflect subtle changes in atmospheric circulation, which need not be associated with a large change in climate. Here we present results from a new Greenland ice core (GISP2) showing that snow accumulation doubled rapidly from the Younger Dryas event to the subsequent Preboreal interval, possibly in one to three years. We also find that the accumulation-rate change from the Oldest Dryas to the Bø11ing/Allerød warm period was large and abrupt. The extreme rapidity of these changes in a variable that directly represents regional climate implies that the events at the end of the last glaciation may have been responses to some kind of threshold or trigger in the North Atlantic climate system.

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Metadata

Authors
Alley, R. B., Meese, D. A., Shuman, C. A., Gow, A. J., Taylor, K. C., Grootes, P. M., White, J. W. C., Ram, M., Waddington, E. D., Mayewski, P. A., & Zielinski, G. A.
Venue
Nature
Published
1993-04
Volume
362
Issue
6420
Pages
527-529
ISSN
  • 0028-0836 (ISSN-L)
  • 1476-4687
OpenAlex
W1975725752
Cited by
1,206
References
17
FWCI
45.90
Type
journal article
Language
en
Open access
green

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CoChat. (2026). Citation check: Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas event. https://app.cochat.ai/papers/10.1038/362527a0
The paper
Alley, R. B., Meese, D. A., Shuman, C. A., Gow, A. J., Taylor, K. C., Grootes, P. M., White, J. W. C., Ram, M., Waddington, E. D., Mayewski, P. A., & Zielinski, G. A. (1993). Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas event. Nature. https://doi.org/10.1038/362527a0

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